Névé Nunatak
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Névé Nunatak
Névé Nunatak () is an isolated nunatak just north of Halfway Nunatak, between the Upper Staircase and the east side of Skelton Névé. Surveyed in 1957 by the New Zealand Northern Survey party of the Commonwealth Trans-Antarctic Expedition The Commonwealth Trans-Antarctic Expedition (CTAE) of 1955–1958 was a Commonwealth-sponsored expedition that successfully completed the first overland crossing of Antarctica, via the South Pole. It was the first expedition to reach the South ... (1956–58) and named for its association with Skelton Névé. Nunataks of the Ross Dependency Hillary Coast {{RossDependency-geo-stub ...
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Nunatak
A nunatak (from Inuit ''nunataq'') is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They are also called glacial islands. Examples are natural pyramidal peaks. When rounded by glacial action, smaller rock promontories may be referred to as rognons. The word is of Greenlandic origin and has been used in English since the 1870s. Description The term is typically used in areas where a permanent ice sheet is present and the nunataks protrude above the sheet.J. J. Zeeberg, ''Climate and Glacial History of the Novaya Zemlya Archipelago, Russian Arctic''. pp. 82–84 Nunataks present readily identifiable landmark reference points in glaciers or ice caps and are often named. While some nunataks are isolated, sometimes they form dense clusters, such as Queen Louise Land in Greenland. Nunataks are generally angular and jagged, which hampers the formation of glacial ice on their tops, although snow can a ...
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Halfway Nunatak
Halfway Nunatak () is an isolated nunatak in the Antarctica, on the west side of The Landing, and almost in the center of the upper Skelton Glacier. It was surveyed and descriptively named in 1957 by the New Zealand party of the Commonwealth Trans-Antarctic Expedition The Commonwealth Trans-Antarctic Expedition (CTAE) of 1955–1958 was a Commonwealth-sponsored expedition that successfully completed the first overland crossing of Antarctica, via the South Pole. It was the first expedition to reach the South ..., 1956–58. See also * Baumann Crag * Schulz Crag References Nunataks of the Ross Dependency Hillary Coast {{RossDependency-geo-stub ...
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Upper Staircase
Skelton Glacier is a large glacier flowing from the polar plateau into the Ross Ice Shelf at Skelton Inlet on the Hillary Coast, south of Victoria Land, Antarctica. Discovery and naming Named after the Skelton Inlet by the New Zealand party of the CTAE, 1956–58. The glacier was chosen in 1957 as the New Zealand party's route from the Ross Ice Shelf to the polar plateau in support of the main expedition led by Vivian Fuchs to make the first overland crossing of the continent. Allison Glacier descends from the west slopes of Royal Society Range into Skelton Glacier. It was also the route of the four month Victoria Land Traverse 1959-1960 which ascended the Skelton Glacier from the Ross Ice Shelf to make the first entry into the deep interior of Victoria Land from the head of the Skelton Glacier to the French Adelie Land Traverse of 1958-1959 near Dumont d'Urville Station on George V Coast, and thence to the Transantarctic Mountains in the vicinity of the USARP Mountains. ...
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Skelton Névé
Skelton Glacier is a large glacier flowing from the polar plateau into the Ross Ice Shelf at Skelton Inlet on the Hillary Coast, south of Victoria Land, Antarctica. Discovery and naming Named after the Skelton Inlet by the New Zealand party of the CTAE, 1956–58. The glacier was chosen in 1957 as the New Zealand party's route from the Ross Ice Shelf to the polar plateau in support of the main expedition led by Vivian Fuchs to make the first overland crossing of the continent. Allison Glacier descends from the west slopes of Royal Society Range into Skelton Glacier. It was also the route of the four month Victoria Land Traverse 1959-1960 which ascended the Skelton Glacier from the Ross Ice Shelf to make the first entry into the deep interior of Victoria Land from the head of the Skelton Glacier to the French Adelie Land Traverse of 1958-1959 near Dumont d'Urville Station on George V Coast, and thence to the Transantarctic Mountains in the vicinity of the USARP Mountains. See ...
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New Zealand Northern Survey
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Commonwealth Trans-Antarctic Expedition
The Commonwealth Trans-Antarctic Expedition (CTAE) of 1955–1958 was a Commonwealth-sponsored expedition that successfully completed the first overland crossing of Antarctica, via the South Pole. It was the first expedition to reach the South Pole overland for 46 years, preceded only by Amundsen's expedition and Scott's expedition in 1911 and 1912. In keeping with the tradition of polar expeditions of the Heroic Age of Antarctic Exploration, the CTAE was a private venture, though it was supported by the governments of the United Kingdom, New Zealand, United States, Australia and South Africa, as well as many corporate and individual donations, under the patronage of Queen Elizabeth II. It was headed by British explorer Vivian Fuchs, with New Zealander Sir Edmund Hillary leading the New Zealand Ross Sea Support team. The New Zealand party included scientists participating in International Geophysical Year research while the British team were separately based at Halley Ba ...
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Nunataks Of The Ross Dependency
A nunatak (from Inuit ''nunataq'') is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They are also called glacial islands. Examples are natural pyramidal peaks. When rounded by glacial action, smaller rock promontories may be referred to as rognons. The word is of Greenlandic origin and has been used in English since the 1870s. Description The term is typically used in areas where a permanent ice sheet is present and the nunataks protrude above the sheet.J. J. Zeeberg, ''Climate and Glacial History of the Novaya Zemlya Archipelago, Russian Arctic''. pp. 82–84 Nunataks present readily identifiable landmark reference points in glaciers or ice caps and are often named. While some nunataks are isolated, sometimes they form dense clusters, such as Queen Louise Land in Greenland. Nunataks are generally angular and jagged, which hampers the formation of glacial ice on their tops, although snow can a ...
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